Difference between revisions of "Cs382"
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=== Activities in Manual === | === Activities in Manual === |
Revision as of 21:15, 31 October 2007
This page documents the work of CS382 - Scientific Computing, Fall 2007
Contents
enVision Tabletop Groundwater Simulator
General Instructions
- Setup
- Teardown and cleaning
- Packing and travelling
Instructions for Demonstrations
- First one
- Second one
- etc.
Computational Groundwater Simulations
Fitz and Bryan
- Replace this with the first experiment
- Replace this with the second experiment
- Replace this with the third experiment
Peter and Mikio
- Replace this with the first experiment
- Replace this with the second experiment
- Replace this with the third experiment
Brad and Nate
Our goal is an incremental approach towards illustrating groundwater contamination in a confined aquifer. The confined aquifer, viewed between wells 1 and 8, offers an environment within the groundwater simulator with the fewest variables. The first 3 experiments are an effort to illustrate the behavior and underlying science that must be understood and demonstrated in the final experiment.
- Diffusion
- Show diffusion without groundwater movement.
- Flow Rate
- Show the leading edge of groundwater contamination as a indicator of flow rate (related to section 5 and 13 in manual)
- Contaminant Plume Length
- Determine whether contaminant plume length is affected by flow rate for a given amount of dye
- Illustrate laminar flow in a confined aquifer (Activity 7-1)
- Show laminar flow between wells 1 and 8.
- Computational Tools
- NetLogo
- + Visualization built in
- + Agent and cell based simulation structure built in
- - Possible limitation on world size / agent count in RAM
- - Possible run time slower than groundwater simulator at higher flow rates
- - Not parallel
- Python and MYMPI
- + Parallelizable
- + Faster than NetLogo in serial code ?
- + Visualization software exists
- - Visualization software must be integrated
- - MYMPI is untested
- NetLogo
Activities in Manual
- Level I: Teaching Basic Groundwater Facts and Concepts with the Model
- 2-1: Demonstrating porosity
- 2-2: Porosity demonstrations
- 3-1: Illustrating the water table (groundwater not flowing)
- 3-2: Illustrating the water table (groundwater flowing)
- 3-3: Raising and lowering the water table
- 4-1: Describing recharge, transition and discharge areas
- 5-1: Describing the slope on the water table (hydraulic gradient)
- 6-1: Observing water level differences in wells in recharge and discharge areas
- 6-2: Potentiometric surfaces
- 7-1: Illustrating groundwater flow in a confined aquifer
- 7-2: Groundwater flow in an unconfined (water table) aquifer
- 8-1: Illustrating and describing groundwater contamination
- 9-1: Pump and Treat, How to operate the syringe system
- 9-2: In-situ treatment
- Level II: Using the Groundwater Model (Elementary - Middle School)
- 10-1: Describing the model
- 11-1: Illustrating and calculating porosity
- 12-1: Estimating the permeability of soils
- 12-2: Graphing the permeability of soils
- 12-3: Determining the actual permeability (MS)
- 12-4: Illustrating the water table
- 12-5: Explaining the water levels in water wells
- 12-6 Explaining a sloping water table
- 12-7 Determine the amount of water (discharge) flowing through the model
- 14-1: Demonstration illustrating what happens when contaminants in groundwater have densities that differ from groundwater
- 14-2: Illustrating how water wells are contaminated
- 14-3: Illustrating the effect of pumping wells on contaminated aquifers
- 14-4: Illustrating how contaminant concentrations can be changed in groundwater